Durrani Taimoor Shah, Akhtar Malik Muhammad, Kakar Kaleem U, Khan Muhammad Najam, Muhammad Faiz, Khan Maqbool, Habibullah H, Khan Changaiz
Department of Environmental Management and Policy, Balochistan University of Information Technology Engineering and Management Sciences (BUITEMS), Quetta, Pakistan.
Department of Environmental Science, Balochistan University of Information Technology Engineering and Management Sciences (BUITEMS), Quetta, Pakistan.
Environ Geochem Health. 2024 Dec 24;47(2):32. doi: 10.1007/s10653-024-02335-2.
Around 2.6 billion people are at risk of tooth carries and fluorosis worldwide. Quetta is the worst affected district in Balochistan plateau. Endemic abnormal groundwater fluoride ( ) lacks spatiotemporal studies. This research integrates geospatial distribution, geochemical signatures, and data driven method for evaluating levels and population at risk. Groundwater ranged from 0 to 3.4 mg/l in (n = 100) with 52% samples found unfit for drinking. Through geospatial IDW tool hotspot areas affected with low and high groundwater levels were identified. Geochemical distribution in geological setups recognized sediment variation leads to high (NaHCO) and low (CaHCO) water types in low elevation (central plain) and high elevation (mountain foot) respectively. Results of the modified water quality index identified 60% samples to be unsuitable for drinking. Support vector machine (SVM), random forest regression (RFR) and classification and regression tree (CART) machine learning models found , Salinity and as important contributing variables in groundwater prediction. CART model with R value of 0.732 outperformed RFR and SVM in predicting . Noncarcinogenic health risk vulnerability from increased from Adults < Teens < Children < Infants. Infants and children with hazard quotient values of 11.3 and 4.2 were the most vulnerable population at risk for consuming contaminated groundwater. The research emphasizes on both nutritional need and hazardous effect of , and development of desirable limit for .
全球约有26亿人面临龋齿和氟中毒的风险。奎达是俾路支斯坦高原受影响最严重的地区。地方性异常地下水氟( )缺乏时空研究。本研究整合地理空间分布、地球化学特征和数据驱动方法来评估氟含量水平和受影响人群。100个样本的地下水中氟含量范围为0至3.4毫克/升,52%的样本被发现不适合饮用。通过地理空间反距离加权(IDW)工具,确定了受低氟和高氟地下水位影响的热点区域。地质构造中的地球化学分布表明,沉积物变化分别导致低海拔(中部平原)的高氟(碳酸氢钠型)水和高海拔(山脚)的低氟(碳酸氢钙型)水。修正后的水质指数结果表明,60%的样本不适合饮用。支持向量机(SVM)、随机森林回归(RFR)和分类回归树(CART)机器学习模型发现,氟、盐度和 是地下水氟预测的重要影响变量。R值为0.732的CART模型在预测氟方面优于RFR和SVM。氟导致的非致癌健康风险脆弱性从成年人<青少年<儿童<婴儿递增。危险商数分别为11.3和4.2的婴儿和儿童是饮用氟污染地下水风险最高的最脆弱人群。该研究强调了氟的营养需求和有害影响,以及确定氟的适宜限量。